A quantitative magnetospheric model derived from spacecraft magnetometer data

作者: Gilbert D. Mead , Donald H. Fairfield

DOI: 10.1029/JA080I004P00523

关键词: PhysicsScalar potentialVector fieldMagnetic fieldL-shellGeodesyComputational physicsCurl (mathematics)MagnetosphereDipole model of the Earth's magnetic fieldField lineEarth-Surface ProcessesEcology (disciplines)Earth and Planetary Sciences (miscellaneous)Space and Planetary SciencePalaeontologyForestryAquatic scienceAtmospheric ScienceSoil scienceGeochemistry and PetrologyGeophysicsOceanographyWater Science and Technology

摘要: A quantitative model of the external magnetospheric field has been derived by making least squares fits to magnetic measurements from four Imp satellites. The data set consists 12,616 vector averages over half-earth radii intervals between 4 and 17 RE, taken 451 satellite orbits 1966 1972. were fit a power series expansion in solar coordinates wind-dipole tilt angle, thus contains effects seasonal north-south asymmetries. is divergence free, but unlike usual scalar potential expansion, nonzero curl representing currents distributed within magnetosphere. includes sets coefficients, different degrees disturbance as determined range Kp values. latitude at earth separating open polar cap lines closing on day side about 5° lower than that previous theoretically models. At times high Kp, additional high-latitude extend back into tail. Near solstice, separation can be low 75° winter hemisphere. average northward component much smaller predicted theoretical models; this finding indicates important Current densities implied are order 10−9 A/m² across magnetotail.

参考文章(35)
V.P. Shabanskii, A.E. Antonova, Structure of the Geomagnetic Field at Great Distances from the Earth Geomagnetism and Aeronomy. ,vol. 8, pp. 639- ,(1968)
M. Sugiura, The ring current. ,(1972)
W. P. Olson, A model of the distributed magnetospheric currents Journal of Geophysical Research. ,vol. 79, pp. 3731- 3738 ,(1974) , 10.1029/JA079I025P03731
Edward W. Hones, Motions of charged particles trapped in the Earth's magnetosphere Journal of Geophysical Research. ,vol. 68, pp. 1209- 1219 ,(1963) , 10.1029/JZ068I005P01209
Gilbert D. Mead, David B. Beard, Shape of the geomagnetic field solar wind boundary Journal of Geophysical Research. ,vol. 69, pp. 1169- 1179 ,(1964) , 10.1029/JZ069I007P01169
GilbertD. Mead, Neutral points on the boundary of the closed magnetosphere Space Science Reviews. ,vol. 7, pp. 158- 165 ,(1967) , 10.1007/BF00215593
W. D. Cummings, P. J. Coleman, G. L. Siscoe, Quiet day magnetic field at ATS 1 Journal of Geophysical Research. ,vol. 76, pp. 926- 932 ,(1971) , 10.1029/JA076I004P00926
Donald J. Williams, Gilbert D. Mead, Nightside magnetosphere configuration as obtained from trapped electrons at 1100 kilometers Journal of Geophysical Research. ,vol. 70, pp. 3017- 3029 ,(1965) , 10.1029/JZ070I013P03017
Joseph C. Cain, Ronald E. Sweeney, Magnetic field mapping of the inner magnetosphere Journal of Geophysical Research. ,vol. 75, pp. 4360- 4362 ,(1970) , 10.1029/JA075I022P04360